The Eurasia Proceedings of Science, Technology, Engineering & Mathematics (EPSTEM)
ISSN: 2602-3199
- This is an Open Access article distributed under the terms of the Creative Commons Attribution-Noncommercial 4.0 Unported License,
permitting all non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.
- Selection and peer-review under responsibility of the Organizing Committee of the conference
*Corresponding author: Ayse Bengu Sunbul-E-mail: [email protected]
© 2017 Published by ISRES Publishing: www.isres.org
The Eurasia Proceedings of Science, Technology, Engineering & Mathematics (EPSTEM)
Volume 1, Pages 388-396
ICONTES2017: International Conference on Technology, Engineering and Science
A CASE STUDY ON 3D NON-LINEAR ANALYSIS OF A CLAY CORE
ROCKFILL DAM
Ayse Bengu Sunbul
Bulent Ecevit University
Murat Cavusli
Bulent Ecevit University
Murat Emre Kartal
Izmir Demokrasi University
Fatih Sunbul
Ulster University
Abstract: Clay core rockfill (CCR) dams are commonly used and the chosen model dam construction due to
their low cost and rapid construction advantages; moreover playing a key role in national water and power
management systems. In terms of large water reservoir impoundment behind a high dam, they include a risk to
the public, in case of an earthquake, especially for urban areas. Therefore, the stability of dam embankment and
analysing seismic safety is of great concern to geotechnical engineers. In fact, these analyses are complex issues
which concern both elastic and dynamic effects on the influence of the seismic response to real earthquake
records. The objective of this study is to evaluate the three dimensional static and dynamic degrading behaviour
of a CCR dam through using the finite difference method. The static part of the analysis considers the layered
construction, reservoir impoundment and vertical displacements whereas, the dynamic part considers the
response of the dam to a real earthquake recording which represents the typical measures of a peak ground
acceleration (PGA) of the study area. Dams should be designed in considering an extreme earthquake with
maximum intensity values. In view of this we have investigated the 3D non-linear seismic behaviour of a CCR
dam which was subjected to the 1999 Mw 7.1 Duzce earthquake and this is consistent with the idea of an
extreme earthquake of about maximum intensity in structural seismic response analysis. The mechanical
behavior of the dam material was described using the Mohr–Coulomb failure criterion. Dynamic analyses of the
model are performed and the dam behaviour and possible failure phenomena presented. Discussions and
comparisons between the non-linear simulation results and existing parameters are expressed.
Keywords: 3D, rockfıll dam, earthquake
Introduction Dams have become a fundamental part of a Nation’s infrastructural body and play an important and beneficial
role in the management and development of water in river basins. The use of clay-core rockfill (CCR) dam
which is constructed with the optimum use of different geotechnical materials with a permanent clay core, is a
preferred model due to its economic reasons. In terms of large water reservoir impoundment behind a high dam,
they include risks to the public, especially for urban areas (USCOLD, 1992). In order to assess these risks
realistically for both static and dynamic states, finite element (FE) technique and finite difference method (FDM)
are the available tools used in the prediction of structural behaviour.
Several researchers have conducted analysis of various types of dams using the FEM. Westergaard (1933)
proposed one of the earliest results of the effect of reservoir on the dam based on some assumptions that, water is
incompressible; dam is rigid with a vertical face. Fok and Chopra (1985) studied the seismic response of a dam
International Conference on Technology, Engineering and Science(ICONTES) October 26 - 29, 2017 Antalya/Turkey
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by means of absorbing boundary conditions. In the review paper by Hall (1988), the importance of both static
and dynamic analyses was explained in detail. Later studies have shown the importance of 2D and 3D FEM
modelling (e.g. Özkan, Özyazicioglu ve Aksar, 2006; Siyahi and Aslan, 2008a and 2008b; Akkose and Simsek,
2010; Kartal, 2012; Ghaedi et al., 2013). Liu et al. (2016) investigated stress, deformation and settlement
analysis of a cut-off wall in a clay core rockfill dam on thick overburden. The results show that selecting plastic
concrete with a low modulus can provide high strength of the clay core of the dam and optimize the connection
between the cut-off walls which decrease the deformation. Rashidi et al. (2017) evaluated the behavior of
rockfill dams during construction and initial impoundment using numerical modeling and instrumentation data.
They also recorded 6 years displacement values and those values showed that the most of the settlement took
place in dam construction phase compared to the following 6 years period.
Stability is expressed in terms of an overall factor of safety. Progress in the area of geotechnical numerical
modelling provide us significant results in the dam physical analysis, in considering complexity such as non-
linear behavior modelling, the evolution of the pore pressure during the construction phase and seismic loading
under real earthquake data. In fact, the determination of earthquake ground motions is a key issue for the
evaluation of the seismic safety of a dam. Seismic ground motions, at a specific dam site, are usually defined in
terms of peak ground acceleration (PGA). PGA is the highest intensity of ground motions recorded by the
seismograms. Since it is not possible to predict the seismic hazard of a given region, geotechnical engineers
consider the maximum intensity in their structural seismic response models.
The paper presents a numerical study of both static and dynamic behaviour of a clay core rockfill dam. All
analyses are conducted using a 3D finite difference modelling. Results are presented first considering static
analyses including layered constructions, reservoir impoundment and predicted vertical displacements in a
selected CCR dam; then analyses are conducted within the framework of non-linearity in vertical displacements
in order on evaluate the influence of water reservoir on the seismic response of the dam.
Modellıng
The non-linear analyses which include elasto-plastic (EPNL) and direct non-linear solutions are conducted using
the finite difference program FLAC3D. FLAC 3D is a direct finite difference program include constitutive
equations, which are elucidated gradually by regular degrees of modelling that allows large strain computations,
material anisotropies and other non-linearities. For dam analysis, the Mohr-Coulomb model is applicable as a
constitutive step (FLAC3D, 2005). Other models are also implemented into the program’s flowchart by using
programming language. At every computing step in the flowchart, incremental strains are calculated in each
elementary zone and result in gradual increase of stress derived from the relevant constitutive equations. These
steps are followed by an update in zone stress and gridpoint displacements (Roth et al. 1991; Dawson et al.
2001). Seismic loading is applied at the base of the foundation layer as a velocity excitation. The Free-field
boundaries procedure in FLAC3D aims absorbing outward waves arise from the structure. FLAC3D contains an
optional form of damping, hysteretic damping, that incorporates strain-dependent damping ratio and secant
modulus functions, allowing direct comparisons between the equivalent-linear method and the fully non-linear
method (FLAC3D, 2005). We followed the same approach in our analysis.
The example model, used in the analyses, is assumed as 35 m in height. The dam has a crest length of 225 m and
a crest width of 10 m. It was considered to store 638.000 m3 of water at maximum capacity (Fig. 1).
Figure 1. Typical cross-section of the CCR dam used in the study
Numerical methods that have been commonly used to assess the dynamic behaviour of dams mainly include the
finite element or finite difference methods-based calculations. In these calculations the non-linear analysis
International Conference on Technology, Engineering and Science(ICONTES) October 26 - 29, 2017 Antalya/Turkey
390
provides the analytical basis of the study which represents the real behaviour of the soil under static
(gravitational) and dynamic loadings. In this study, we have used non-linear approach which provides a more
complete insight of the behaviour of the clay core rockfill dams and finally contribute to reach the realistic
output of the dynamic analysis. The selected material parameters for the dam are shown in Table 1.
Table 1. Foundation and soil properties used in the geotechnical analyses.
Material Properties
Material Maximum
Unit
Weight
Young’s
modulus
Cohesion Internal
friction angle
Dilation
angle
Poisson’s
Ratio
Clay Core 1.59 21 MPa 50 kPa 26° 0 0.32
Rockfill 1.99 45 MPa 0 37° 8 0.28
Gravel Filter 2.15 32 MPa 0 34° 4 0.30
Sand Filter 2.14 29 MPa 0 32° 3 0.30
Rock Pieces Filter 2.16 34 MPa 0 33° 4 0.29
Foundation 2.25 10 GPa 0 42° 10 0.25
The dam with its foundation (down to 35 m) was modelled by generating brick type zones. The free-field
boundaries procedure in FLAC3D is used in order to aim absorbing outward waves arise from the dam structure.
Assuming the height of dam as h; we extend the reservoir length up to 3h which is consistent to acquire more
realistic results in the seismic response of a dam (e.g. Bayraktar et al., 2012; Kartal et al., 2017). The dam’s
body is carried out of clay, with slope inclination of 1:2.5 upstream and 1:2.0 downstream. Filter material in both
sides of the dam is carried out of rock, gravel and sand, with slope inclination of 1:0.5 (Fig. 2).
Figure 2. The dam is assumed as having asymmetric zone sections (h: downstream length, 3h: upstream length)
with clay core and foundation (See also Table 1 for material properties used in the analysis)
In fact, the two third of Turkey, being located in a 2nd degree earthquake zone according to the Ministry of
Public works and Settlement, General Directorate of disaster affairs report (AFAD, 2016). Dams should be
designed in considering an extreme earthquake with maximum intensity values. In view of this we have
investigated the 3D non-linear seismic behaviour of the CCR dam which was subjected to the 1999 Mw 7.1
Duzce earthquake and this is consistent with the idea of an extreme earthquake of about maximum intensity in
structural seismic response analysis. Therefore, we defined the construction area as a 2nd degree earthquake zone
in our scenario that, this area has the probability to produce up to 0.4 g peak ground acceleration (PGA) value.
Therefore, the example model is subjected to the 1999 Mw 7.1 Duzce Earthquake strong ground motion data
which had 0.4 g PGA value (Fig. 3).
X
Y
Z
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391
Figure 3. The 1999 Mw 7.1 Duzce earthquake accelerogram
Results Analyses were conducted in three steps in order to assess the vertical displacements. These steps include static or
dynamic analyses of vertical displacements during; a) dam’s construction phase, b) full water reservoir phase
and c) seismic excitations under real earthquake data. Three observation points (three element integration points:
PA, PB and PC), for which the time history graphs of the response quantities are plotted, are marked on the mesh
as shown in Fig. 4.
Figure 4. Mesh model presented in a cross-section with three observation points
Construction Phase
The static solutions of the dam empty-reservoir system due to its gravity load are shown in Figure 5. The
software has modelled the dam’s gravity load in 1500 steps. It is obvious that the maximum predicted
displacement values are obtained at the top of the clay core (PA) with the value of 12 cm. The vertical
displacements in this phase, are constantly increasing until the 500th step during the analysis. From this point on,
the displacements have become constant. When the other two points (PB and PC) in the dam body are examined,
the predicted vertical displacement of about 4.5 cm obtained at PB while that value is about 1.5 cm at PC. In
general, it was observed that vertical displacement values at the points near the clay core were higher than those
at the other points, and vertical displacements decreased as the distance from the clay core increased.
PA PB
PC
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Figure 5. Vertical displacements at PA, PB and PC during construction phase
Figure 6 shows the contour diagram of the vertical displacements values obtained from static analysis in
construction phase. It is observed that the maximum displacement value is 21.59 cm in the clay core of the dam.
It has been also deduced that the vertical displacement values have decreased according to the direction from
core to the outer filter layers, the value reaches down to 5 cm.
Figure 6. Contour plot of vertical displacements during construction phase
Impounding Phase
The static analyses were also carried out for impounding phase. The reservoir water with an elevation of 35
meters was included in the model using applied pressures to the surface of the reservoir bottom and dam. During
impounding, the hydrostatic force acts on the surface of the dam body. It is assumed that the hydrostatic force is
zero at the top the dam body. The direction and the magnitude of the hydrostatic forces during the impoundment
phase are shown as arrows in Fig. 7.
FLAC3D 3.00
Itasca Consulting Group, Inc.Minneapolis, MN USA
Step 1556 Model Perspective23:15:49 Wed Sep 27 2017
Center: X: 1.194e+001 Y: 1.276e+002 Z: 2.500e-001
Rotation: X: 30.000 Y: 0.000 Z: 30.000
Dist: 1.109e+003 Mag.: 1.25Ang.: 22.500
Plane Origin: X: 0.000e+000 Y: 9.825e+001 Z: 0.000e+000
Plane Orientation: Dip: 90.000 DD: 0.000
Contour of Z-Displacement Plane: on behind Magfac = 0.000e+000
-2.1597e-001 to -2.1500e-001-2.0500e-001 to -2.0000e-001-1.9000e-001 to -1.8500e-001-1.7500e-001 to -1.7000e-001-1.6000e-001 to -1.5500e-001-1.4500e-001 to -1.4000e-001-1.3000e-001 to -1.2500e-001-1.1500e-001 to -1.1000e-001-1.0000e-001 to -9.5000e-002-8.5000e-002 to -8.0000e-002-7.0000e-002 to -6.5000e-002-5.5000e-002 to -5.0000e-002
FLAC3D 3.00
Itasca Consulting Group, Inc.Minneapolis, MN USA
Step 1556 Model Perspective23:15:49 Wed Sep 27 2017
Center: X: 1.194e+001 Y: 1.276e+002 Z: 2.500e-001
Rotation: X: 30.000 Y: 0.000 Z: 30.000
Dist: 1.109e+003 Mag.: 1.25Ang.: 22.500
Plane Origin: X: 0.000e+000 Y: 9.825e+001 Z: 0.000e+000
Plane Orientation: Dip: 90.000 DD: 0.000
Contour of Z-Displacement Plane: on behind Magfac = 0.000e+000
-2.1597e-001 to -2.1500e-001-2.0500e-001 to -2.0000e-001-1.9000e-001 to -1.8500e-001-1.7500e-001 to -1.7000e-001-1.6000e-001 to -1.5500e-001-1.4500e-001 to -1.4000e-001-1.3000e-001 to -1.2500e-001-1.1500e-001 to -1.1000e-001-1.0000e-001 to -9.5000e-002-8.5000e-002 to -8.0000e-002-7.0000e-002 to -6.5000e-002-5.5000e-002 to -5.0000e-002
Contour of Z displacement
Empty reservoir state
Displacements (cm)
International Conference on Technology, Engineering and Science(ICONTES) October 26 - 29, 2017 Antalya/Turkey
393
Figure 7. Meshing of the dam model; the hydrostatic force is shown as vectors
Figure 8 shows the non-linear time-history graph of the vertical displacement at PA, PB and PC during full water
reservoir phase. The maximum displacement values are observed at the dam’s crest up to 18 cm. The vertical
displacements obtained at the crest are continuously increasing up to 500th step and the value become more
stable after that point. At PB and PC, vertical displacements of 11.5 cm and 6.5 cm were calculated, respectively.
According to the predicted data, the largest displacement occurred in the clay core, which is the weakest material
of the dam body. Moreover, when the empty state and the full water state of the dam are compared, it has been
observed that the vertical displacement values occurring at the crest point of the dam increase depending on the
reservoir water. Furthermore, after starting impounding stage, it was observed that the vertical displacements
were visibly increased due to the hydrostatic pressure acting on the points B and C.
The influence of the variation of the water level in the reservoir is also compared. In both cases (empty and full
water reservoir states), we obtain higher displacement variations at PA when compared to PB and PC.
Figure 8. Vertical displacements at PA, PB and PC during impounding phase
Figure 9 shows the contour diagram of vertical displacements obtained at the dam’s body during the
impoundment phase. The maximum vertical displacement occurs at dam clay core with magnitude 41 cm. In
terms of displacement values over the filter layers; we obtained displacement with magnitude 17 cm due to
hydrostatic pressure. This value is higher than those obtained in the empty reservoir phase. The results are in
good agreement with previous studies (Parish, 2007).
International Conference on Technology, Engineering and Science(ICONTES) October 26 - 29, 2017 Antalya/Turkey
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Figure 9. Contour plot of vertical displacements during the impounding phase
Dynamic Phase
Fig. 10 shows the vertical displacement time history of the dam under seismic loading for 15 sec. The maximum
displacement occurs at dam crest (PA) with magnitude 86 cm. Those values decrease down to 45 cm at PA and
PB. The peak values are observed in the strong ground motion record in the first 5 sec period. After that time
period, we observe continuous displacement values where the residual deformations are being estimated. The
higher predicted displacements are also observed at PC when compared to PB.
Figure 10. Vertical displacements at PA, PB and PC during seismic excitation phase
Fig. 11 shows the dynamic response of the dam under earthquake loading. From Fig 11, displacement responses
increase gradually from bottom to top and displacement response of dam crest are larger than those observed at
the dam foot.
FLAC3D 3.00
Itasca Consulting Group, Inc.Minneapolis, MN USA
Step 2680 Model Perspective23:26:50 Wed Sep 27 2017
Center: X: 4.250e+001 Y: 1.100e+002 Z: 2.500e-001
Rotation: X: 30.000 Y: 0.000 Z: 30.000
Dist: 1.109e+003 Mag.: 1.25Ang.: 22.500
Plane Origin: X: 0.000e+000 Y: 9.825e+001 Z: 0.000e+000
Plane Normal: X: 0.000e+000 Y: 1.000e+000 Z: 6.123e-017
Contour of Z-Displacement Plane: on behind Magfac = 0.000e+000
-4.1160e-001 to -4.1000e-001-3.8500e-001 to -3.8000e-001-3.5500e-001 to -3.5000e-001-3.2500e-001 to -3.2000e-001-2.9500e-001 to -2.9000e-001-2.6500e-001 to -2.6000e-001-2.3500e-001 to -2.3000e-001-2.0500e-001 to -2.0000e-001-1.7500e-001 to -1.7000e-001-1.4500e-001 to -1.4000e-001-1.1500e-001 to -1.1000e-001-8.5000e-002 to -8.0000e-002
FLAC3D 3.00
Itasca Consulting Group, Inc.Minneapolis, MN USA
Step 2680 Model Perspective23:26:50 Wed Sep 27 2017
Center: X: 4.250e+001 Y: 1.100e+002 Z: 2.500e-001
Rotation: X: 30.000 Y: 0.000 Z: 30.000
Dist: 1.109e+003 Mag.: 1.25Ang.: 22.500
Plane Origin: X: 0.000e+000 Y: 9.825e+001 Z: 0.000e+000
Plane Normal: X: 0.000e+000 Y: 1.000e+000 Z: 6.123e-017
Contour of Z-Displacement Plane: on behind Magfac = 0.000e+000
-4.1160e-001 to -4.1000e-001-3.8500e-001 to -3.8000e-001-3.5500e-001 to -3.5000e-001-3.2500e-001 to -3.2000e-001-2.9500e-001 to -2.9000e-001-2.6500e-001 to -2.6000e-001-2.3500e-001 to -2.3000e-001-2.0500e-001 to -2.0000e-001-1.7500e-001 to -1.7000e-001-1.4500e-001 to -1.4000e-001-1.1500e-001 to -1.1000e-001-8.5000e-002 to -8.0000e-002
Contour of Z displacement
Full-water reservoir state
Displacements (cm)
International Conference on Technology, Engineering and Science(ICONTES) October 26 - 29, 2017 Antalya/Turkey
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Figure 11. Contour plot of vertical displacements during seismic excitation phase
Conclusion
In order to assess static and dynamic vertical displacements on a selected CCR dam, three dimensional non-
linear analyses were carried out. The static part of the analysis considers the vertical displacement variations
following construction phase and reservoir impoundment whereas; the dynamic part considers the response of
the dam to a real earthquake recording. The results of this study are summarized as follows;
- During the construction phase (static state); the maximum displacements were observed at the top of the
clay core (crest of the dam). The predicted displacement value was 12 cm at the crest, whereas this
value was gradually decreased in consideration of lower parts of the dam body. The 3D contour
diagram also shows that the displacement value obtained in the clay core was approximately 21.5 cm.
- During the impounding phase (static state); the predicted vertical displacement value observed at the
dam crest was 18 cm and gradually increased towards to the bottom level. The 3D contour diagram for
this case shows the maximum displacement value with magnitude 41 cm at dam clay core.
- The static state analyses show a gradual increase in the magnitude of vertical displacements during an
impounding stage where the hydrostatic force acts on the surface of the dam body and causes additional
force on the clay core section.
- During the dynamic phase; the CCR dam was subjected to the ground acceleration histories obtained by
the 1999 Mw 7.1 Duzce earthquake which had 0.4 g peak acceleration value. The seismic excitation
increased the magnitude of displacements when compared to the static phases. We observe 86 cm
vertical displacement value at the crest of the dam in the first 5 sec of recording. For the rest of seismic
excitement, the residual/permanent deformations have been also observed due to the continuous seismic
loading.
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FLAC3D 3.00
Itasca Consulting Group, Inc.Minneapolis, MN USA
Step 90397 Model Perspective22:38:56 Wed Sep 27 2017
Center: X: 1.781e+001 Y: 1.748e+002 Z: 6.892e+000
Rotation: X: 30.000 Y: 0.000 Z: 30.000
Dist: 1.383e+003 Mag.: 1.56Ang.: 22.500
Plane Origin: X: 0.000e+000 Y: 9.825e+001 Z: 0.000e+000
Plane Orientation: Dip: 90.000 DD: 0.000
Contour of Z-Displacement Plane: on behind Magfac = 1.000e+000
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Itasca Consulting Group, Inc.Minneapolis, MN USA
Step 90397 Model Perspective22:38:56 Wed Sep 27 2017
Center: X: 1.781e+001 Y: 1.748e+002 Z: 6.892e+000
Rotation: X: 30.000 Y: 0.000 Z: 30.000
Dist: 1.383e+003 Mag.: 1.56Ang.: 22.500
Plane Origin: X: 0.000e+000 Y: 9.825e+001 Z: 0.000e+000
Plane Orientation: Dip: 90.000 DD: 0.000
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Full-water reservoir state
Contour of Z displacement
Displacements (cm)
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